蒸腾作用 Transpiration
蒸腾作用(英语:transpiration,或称蒸散作用)是指水分从植物表面散失的现象。水分在植物表面由液体变成气体,这过程需要能量,这能量称为蒸发潜热,在大自然中能量是由太阳供应的。
单词 | Transpiration ratio |
释义 |
Transpiration ratio
中文百科
蒸腾作用 Transpiration(重定向自Transpiration ratio)
蒸腾作用(英语:transpiration,或称蒸散作用)是指水分从植物表面散失的现象。水分在植物表面由液体变成气体,这过程需要能量,这能量称为蒸发潜热,在大自然中能量是由太阳供应的。
英语百科
Transpiration 蒸腾作用(重定向自Transpiration ratio)
![]() ![]() ![]() ![]() Transpiration is the process of water movement through a plant and its evaporation from aerial parts, such as leaves, stems and flowers. Water is necessary for plants but only a small amount of water taken up by the roots is used for growth and metabolism. The remaining 97–99.5% is lost by transpiration and guttation. Leaf surfaces are dotted with pores called stomata, and in most plants they are more numerous on the undersides of the foliage. The stomata are bordered by guard cells and their stomatal accessory cells (together known as stomatal complex) that open and close the pore. Transpiration occurs through the stomatal apertures, and can be thought of as a necessary "cost" associated with the opening of the stomata to allow the diffusion of carbon dioxide gas from the air for photosynthesis. Transpiration also cools plants, changes osmotic pressure of cells, and enables mass flow of mineral nutrients and water from roots to shoots. Two major factors influence the rate of water flow from the soil to the roots: the hydraulic conductivity of the soil and the magnitude of the pressure gradient through the soil. Both of these factors influence the rate of bulk flow of water moving from the roots to the stomatal pores in the leaves via the xylem. |
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